Assessment of Hydrogeological Characteristics & Groundwater Potentiality in Daralsalam Area North Darfur State, Sudan
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Date
2012
Authors
Journal Title
Journal ISSN
Volume Title
Publisher
Neelain University
Abstract
ABSTRACT
Daralasalam area is located laid at 12°:30' -14":30' N and 24°:30'-26°:20' E,
covering (10266 kmz), characterized by undulated surface, arid to semi- arid,
average rainfall (300-195 mm), temperature (11.0 C° — 42.0 C °), relative
humidity (30% - 58%) inhabited by (133782 persons) rely on groundwater. The
study objectives are to assess the Hydro geological characteristics and evaluate
the groundwater potentialities in Daralasalam —North Darfur in Sudan. The
geomorphologic , meteorological, hydrological and hydrogeological,
hydrochemical and geological data, Supported by geophysics, land Sat
imagery for structural analysis map were collected through field
reconnaissance, surveys and office works and analysed by Land Sat imagery
maps enhancement ,GIS techniques, Surfer, C0relDraw soflware —Ph0to Paint,
1Pi2win, Aquitest, AquaChem, and MODFLOW2000 for Ground water
Modeling. Geologically it comprises of basement complex, Cretaceous
Nubian sandstone rocks greater than (371.0 m) thick, intercalated with
basaltic in Shagra and overlain by superficial deposits .Hydro geologically it
consists of Unconfined cretaceous Nubian sandstone aquifers of maximum
hydraulic conductivity and transmissivity was (5.112 m/day) and ( 104.976
m2/day) respectively as the specific yield and the storativity were (45.4%) and
(9.54x 105) respectively. In leaky confined aquifers of basement rocks overlain
by alluvial aquifers the maximum hydraulic conductivity was (9.306 m/day)
and storativity is (7.63x10' ).Chemically it is High TDS , EC, hard , fit for
drinking but poor suitability for irrigation because of high SAR, Na%, EC,
and the C2 Sodium Hazardous. The subsurface flow was (24 M m3/year)
against abstraction of (1 1M m3 /year) while annual balance was (703.oMm3)
and the safe yield was (354130 M m3/year) in Daralasalam area. The
Groundwater Modeling in Shagra basin revealed (175.4 M m3) inflow, (3.9X
105 m3) out flow to balance (l35.7X 105 ma ) during (455days).The assessment
recommended for effective use ensuring safe yield for the current and next
generation
Description
A Thesis Submitted to the Graduate College in Fulfillment of the
Requirements for the Master Degree of Science in Geology
(llydrogeology)
Keywords
Hydrogeological Characteristics
